CRYSTAL-STRUCTURE OF ZEOLITE-A EXCHANGED WITH AG+ AND TL+, AG6.5TL5.5-A, EVACUATED AT 400-DEGREES-C - PARTIAL MECHANISM FOR INTRAZEOLITIC REDUCTION OF AG+ TO FORM HEXASILVER

被引：31

作者：

KIM, Y ^{[1
]}

SEFF, K ^{[1
]}

机构：

[1] UNIV HAWAII,DEPT CHEM,HONOLULU,HI 96822

来源：

JOURNAL OF PHYSICAL CHEMISTRY | 1978年 / 82卷 / 11期

关键词：

D O I：

10.1021/j100500a022

中图分类号：

O64 [物理化学（理论化学）、化学物理学];

学科分类号：

070304 ; 081704 ;

摘要：

引用

页码：1307 / 1311

页数：5

共 27 条

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[7] NEAR-ZERO-COORDINATE THALLIUM(I) - CRYSTAL-STRUCTURES OF HYDRATED AND DEHYDRATED ZEOLITE A FULLY EXCHANGED WITH TIOH
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[8] JOHNSON CK, 1965, ORNL3794 OAK RIDG NA
[9] STRUCTURE OF A VERY SMALL PIECE OF SILVER METAL - OCTAHEDRAL AG6 MOLECULE, 2 CRYSTAL-STRUCTURES OF PARTIALLY DECOMPOSED VACUUM-DEHYDRATED FULLY AG+-EXCHANGED ZEOLITE-A
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SEFF, K
[J]. JOURNAL OF THE AMERICAN CHEMICAL SOCIETY, 1977, 99 (21) : 7055 - 7057
[10] CRYSTAL-STRUCTURE OF A BROMINE SORPTION COMPLEX OF DEHYDRATED FULLY AG+-EXCHANGED ZEOLITE-A
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[J]. JOURNAL OF PHYSICAL CHEMISTRY, 1978, 82 (08) : 925 - 929

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